COS 28-6 - Abiotic and biotic determinants of photosynthetic and respiratory capacity from tropical to high boreal biomes

Tuesday, August 9, 2016: 3:20 PM
Grand Floridian Blrm A, Ft Lauderdale Convention Center
Nicholas G. Smith, Biological Sciences, Purdue University, West Lafayette, IN and Jeffrey S. Dukes, Purdue Climate Change Research Center, Purdue University, West Lafayette, IN
Background/Question/Methods

The Earth System Models (ESMs) that are used to make climate projections are highly sensitive to the parameterization of photosynthetic and respiratory capacity. This stems from the fact that very little research has been done to quantify the primary mechanisms underlying these processes at global scales. Here, we measured the maximum rate of Rubisco carboxylation (Vcmax25), the maximum rate of electron transport (Jmax25), and leaf respiration in dark (Rd25), all standardized to 25°C. In total, we measured 98 species at 12 different American sites spanning 53° of latitude from the neotropics to the high boreal zone. Species sampled encompassed each of the major plant functional types simulated in ESMs. Abiotic and biotic covariate data were collected along with each measurement. We hypothesized that leaf carbon exchange capacity would be positively correlated with leaf nitrogen, as has been observed in previous studies. We also expected faster growing species to have larger capacities. Additionally we hypothesized that increases in recent temperature history would enhance leaf carbon exchange capacity (an acclimation response).

Results/Conclusions

Leaf nitrogen content was the strongest predictor of Vcmax25, Jmax25, and Rd25, with each flux showing strong increases with leaf nitrogen (p<0.05 in all cases). The fluxes were highest in annual compared to perennial plants, broadleaf compared to needleleaf plants, and, for Jmax25 and Rd25, boreal compared to temperate and tropical plants (p<0.05 in all cases). Additional analyses suggested that the effect of climatic region may be due to differences in day length between the sites. Recent temperature history acted to decrease Jmax25 (p<0.05), but had little influence on Vcmax25 or Rd25. The response of the fluxes to soil moisture was generally weak, but an interaction between soil moisture and leaf nitrogen revealed increased Rd25 response to nitrogen in wetter environments, indicating a possible co-limitation of water and nitrogen for Rd25. A comparison of biotic- and abiotic-based models suggested that biotic data (i.e., plant type characteristics) are better for predicting photosynthetic and respiratory capacity than abiotic data. The mechanisms quantified here could be used to improve the parameterizations of plant carbon exchange processes in ESMs.